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Recent X-Ray Structural Work on Serpentine Minerals

Published online by Cambridge University Press:  01 January 2024

J. Zussman
J. Zussman*
Affiliation:
Department of Geology, Manchester University, England
*
1Temporary address: The Pennsylvania State University, University Park, Pennsylvania, USA
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Abstract

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Type
Article
Information
Clays and Clay Minerals (National Conference on Clays and Clay Minerals) , Volume 4 , February 1955 , pp. 80 - 81
Copyright
Copyright © The Clay Minerals Society 1955

References

Brindley, G. W., 1954, X-ray study of a new variety of serpentine (ortho-antigorite): in Clays and clay minerals, Natl. Acad. Sci.—Natl. Res. Council Pub. 327, p. 354–359.Google Scholar
Brindley, G. W., and Von Knorring, O., 1954, A new variety of antigorite (ortho-antigorite) from Unst, Shetland Islands: Amer. Min., v. 39, p. 794–804.Google Scholar
Gruner, J. W., 1937, Notes on the structure of serpentines: Amer. Min., v. 22, p. 97–103.Google Scholar
Midgley, H. G., 1951, A serpentine mineral from Kennack Cove, Lizard, Cornwall: Min. Mag., v. 29, p. 526–530.Google Scholar
Selfridge, G. C. Jr., 1936, An x-ray and optical investigation of the serpentine minerals: Amer. Min., v. 21, p. 463–503.Google Scholar